Minerals of the Earth*s Crust
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Transcript Minerals of the Earth*s Crust
MINERALS OF THE EARTH’S
CRUST
Chapter 1
WHAT IS A MINERAL?
Section 1 Vocabulary
Mineral
Element
Compound
Crystal
Silicate Mineral
Nonsilicate Mineral
THE FOUR ESSENTIAL QUESTIONS
Is it nonliving
material?
Is it a solid?
Does it have a
crystalline structure?
Is it formed in nature?
MINERAL STRUCTURE
Four questions
Crystalline Structure
Needs to be a yes for
all 4
Need to know about
elements
Elements
All minerals contain
one or more
92 naturally occuring
elements
ATOMS AND COMPOUNDS
One kind of element
Atom-smallest part of
an element that has all
the properties of that
element
Compound
Halite-NaCl
Compound
Na-Sodium
Cl-Chlorine
One Element
Gold or Silver
Native element
CRYSTALS
Shape-by the
arrangement of the
atoms within the
crystal
Arrangement-by the
kinds of atoms that
make up the mineral
Definite crystalline
structure
Crystal Classes
TWO GROUPS OF MINERALS
Most common
classification of
minerals is based on
chemical composition
Silicate minerals
Nonsilicate minerals
SILICATE MINERALS
Silicon and oxygen
Two most common
elements in the
Earth’s crust
Combination
90%
Combine with other
elements
NONSILICATE MINERALS
Do not contain silicon
and oxygen
Most important
classes
Native elements
Carbonates
Halides
Oxides
Sulfates
Sulfides
IDENTIFYING MINERALS
Section 2 Vocabulary
Luster
Streak
Cleavage
Fracture
Hardness
Density
COLOR
Same mineral-variety
of colors
Quartz
Granite
Change of color
Impurities
Other factors
Air
Water
NOT THE BEST WAY
TO IDENTIFY A
MINERAL
LUSTER
The way a surface
reflects light
Shiny or dull
Metallic-Shiny, bright,
and reflective
Submetallic-dull and
reflective
Nonmetallic-dull and
not reflective
Figure 1
STREAK
The color of a mineral in
powered form
Streak Plate-a mineral’s
streak can be found by
rubbing the mineral
against a piece of
unglazed porcelain
Color is not always the
same
Not affected by air or
water
MORE RELIABLE
THAN COLOR
CLEAVAGE AND FRACTURE
The way a mineral
breaks is determined
by the arrangement of
its atoms.
Cleavage-break
smooth
Fracture-uneven
break
HARDNESS
A mineral’s resistance to
being scratched
MOHS HARDNESS
SCALE
Talc-1
Diamond-10
The greater a mineral’s
resistance to being
scratched is, the higher
the mineral’s rating is.
Scratch it on another
rock
DENSITY
The measure of how
much matter is in a
given amount of
space.
Density=Mass/Volume
Grams per cubic
centimeter (g/cm3)
Water is used as a
reference point.
1 g/cm3
Specific Gravity
SPECIAL PROPERTIES
Only a few minerals!
Fluorescence-glow
under ultraviolet light
Magnetism-attract
iron
Chemical Reactionacid will cause a fizz
Taste-halite-salty
Optical Propertiesdouble image
Radioactivity- radium
or uranium
THE FORMATION MINING AND USE OF
MINERALS
Section 3 Vocabulary
Ore
Reclamation
MINING
Must be mined to
extract valuable
elements
To describe a mineral
deposit large enough
and pure enough to be
mined for profit
Two Forms
Surface Mining
Subsurface Mining
Depends on Location
SURFACE MINING
At or Near the Surface
Open pits- remove large,
near-surface deposits of
economically important
minerals
Gold/silver
Downward layer by layer
Explosives
Surface Coal Mines-strip
mining-moved in strips
Quarries-used for mining
building stone, crushed
rock, sand, and gravel
SUBSURFACE MINING
Too deep within the
Earth to be surface
mined
Passageways
Horizontally
At an angle
If deep in the earth a
vertical shaft is sunk
Connects passageways
at different levels
RESPONSIBLE MINING
Return the land to its
original state after the
mining is complete
Law since mid-1970’s
Reduce needs for
minerals
Recycling
METALLIC MINERALS
Shiny Surfaces
Does not let light pass
through them
Conductors of heat
and electricity
Strong, Do not Rust
Gold, Silver, and
Copper
NONMETALLIC
Shiny or dull surfaces
May let light pass
through them
Good insulators of
electricity
Most Widely used
Calcite and Silica
GEMSTONES
Highly Valuable
Diamond, Ruby,
Sapphire, etc.
Color is most
important
More attractive the
more value
Durable
Carat